Transparent, terminated Quartz crystal from 1990s finds at Mt. Yaruda. Reportedly one the best, largest crystals from the find with large termination faces that allow an excellent view the chlorite phantoms inside. Comew with a custom made wooden base. Ex. Jeff Glover Quartz collection.

Green scalenohedral Calcite crystals on petrified wood. From a new find.

Thick, glassy crystals of Cerussite from Bunker Hill. This came out of an old collection and was likely found many decades ago. The thick transparent crystals are more reminiscent of material from Tsumeb than Cerussites you would expect from the USA.

Cluster of deep blue Sapphire crystals, translucent along edges. Main crystal is tabular and 2.1cm wide.

Complex intergrown crystals with excellent luster and good brassy color. Solid Pyrite and a little different than the more commonly seen single crystals from the mine.

High quality, glassy crystals with a rich golden color. Undamaged crystals to 8mm in size.

Velvety green Prehnite that formed over (now gone) Anhydrite crystals, leaving this rare and wonderful specimen. Transluscent and undamaged. The inside shows the flat, smooth surfaces of the former Anhydrite crystals.

Layer of solid shattuckite covered by Chrysocolla upon which grew the rare double psuedomorph of Shattuckite after Dioptase after Calcite. Good crystals from the spring of 2011 find. Rare and from a limited find.

Fine quality specimen featuring a 2.8cm blue Tourmaline (var. Indicolite) grwoing from a mound of white Albite. A terminated Quartz crystal balances the specimen on the left side. Complete all around, clean, and undamaged.

Golden yellow Wulfenite crystals to 1.7cm with small spherical Mimetite crystal groupss, good all around.

Silica rich matrix hosting a 1.4cm fossil gastropod that has been replaced by translucent orange Chalcedony. Perfectly preserved and undamaged. This was found in the Morrison formation and is approximately 155 million years old. Collected by Bill Hawes.

Bright yellow crystals of Smithsonite replacing Dolomite, with the curving form of the former Dolomite crystals clearly evident. Smithsonite also covers the surface of the matrix. The bright color is caused by inclusions of Greenockite.

Transparent light green Fluorite cubes with transparent wafer-like Calcite crystals. The quality of both the Fluorite and Calcite is remarkable. The best of a small lot I obtained years ago.